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Geoscience ›› 2018, Vol. 32 ›› Issue (06): 1150-1160.DOI: 10.19657/j.geoscience.1000-8527.2018.06.04

• Petroleum Geology • Previous Articles     Next Articles

Hydrocarbon Distribution Pattern of Superimposed Unconformity Structure: A Case of Carboniferous Donghe Sandstone in Tazhong Area, Tarim Basin, NW China

WANG Tao1,2, XU Huaimin3, DENG Xili4, DONG Shaoqun3, JIANG Tongwen5, ZHOU Xinping6, HUANG Ya3   

  1. 1. Chinese Academy of Geological Sciences, Beijing 100037,China
    2. SinoProbe Center,Chinese Academy of Geological Sciences,Beijing 100037,China
    3. College of Geosciences, China University of Petroleum, Beijing 102249,China
    4. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083,China
    5. PetroChina Tarim Oilfield Company, Korla,Xinjiang 841000,China
    6. PetroChina Changqing Oilfield Company, Xi’an,Shaanxi 710018,China
  • Received:2018-01-05 Revised:2018-05-10 Online:2018-12-10 Published:2018-12-20

Abstract:

In this paper, we discuss: (1) the unconformity types along the Donghe sandstone third-order sequence boundary; (2) different ways of hydrocarbon migration and accumulation caused by space-time orderly distribution of unconformity structures. The Donghe sandstone can be divided into superstratum of the unconformity (bottom), in-place carrier bed, residual regolith, weathered clay bed, superstratum of unconformity (top) and regional cap rock. Pool-forming units are different in the northwest and southeast of the district. They can form 2 groups and 7 types of pool-forming structures, with the former corresponding to two groups of reservoirs. Major structures are separated in the northwest. Hydrocarbon can migrate below the weathered clay bed and regional cap rock, forming the unconformity-blocked reservoir group, including anticlinal reservoir of superstratum of unconformity (top), lithologic reservoirs of superstratum of unconformity (top) and low amplitude anticlinal reservoir of residual regolith. Structures are connected in the southeast, and the hydrocarbon may have migrated below the superstratum of unconformity (bottom) and regional cap rock, forming the unconformity-connected reservoir group, including connected anticlinal- and connected stratigraphic overlap reservoirs. This finding facilitates further hydrocarbon exploration in the Donghe sandstone.

Key words: unconformity, hydrocarbon accumulation type, Donghe sandstone, superimposed unconformity structure, Tazhong area

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